Synchysite-(Ce) is a rare earth carbonate mineral often found in alkaline environments. It is best identified by its distinct tabular, pseudohexagonal habit and typical tan or yellow-brown coloration, frequently occurring with other rare earth minerals.
Is this synchysite-(ce)?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch synchysite-(ce) with a known reference. Synchysite-(Ce) sits at Mohs 4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Synchysite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Synchysite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, gray, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, often pseudohexagonal and flattened.
Often found alongside synchysite-(ce)
Minerals reported to co-occur with synchysite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCe(CO₃)₂F
- Mohs hardness
- 4.5
- Density
- 3.9 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Often Pseudohexagonal and Flattened
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Igneous Rocks, Pegmatites, And Carbonatites
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find synchysite-(ce)
Classic worldwide localities
- Mont Saint-Hilaire, Quebec, Canada
- Narsarsuk, Greenland
- Kola Peninsula, Russia
- Fen Complex, Norway
Field-hunting tip
Look in alkaline igneous rocks, pegmatites, and carbonatites country — that is the host setting where synchysite-(ce) typically forms. If you start seeing aegirine, microcline, fluorite in float, you are in the right ground. Field specimens usually show a tabular crystals, often pseudohexagonal and flattened habit, so train your eye for that shape before scanning the outcrop.





